{"id":8258,"date":"2020-02-02T17:15:06","date_gmt":"2020-02-02T17:15:06","guid":{"rendered":"http:\/\/icelandgeology.net\/?p=8258"},"modified":"2020-02-02T17:15:06","modified_gmt":"2020-02-02T17:15:06","slug":"earthquake-activity-update-for-grindavik-town-2nd-february-2020","status":"publish","type":"post","link":"https:\/\/icelandgeology.net\/?p=8258","title":{"rendered":"Earthquake activity update for Grindav\u00edk town 2nd February 2020"},"content":{"rendered":"<p><strong>Donations<\/strong><br \/>\nPlease remember to support my work with donations. I have removed all the advertisements because of increased tracking with those advertisements and almost no income from them. That means I am more dependant on donation to keep this website running. This is also important in times when there is a lot going on in Iceland as now. Thanks for the support. \ud83d\ude42<\/p>\n<p><strong>Earthquake update for 2nd February 2020<\/strong><\/p>\n<p>Earthquake activity close to Grindav\u00edk town continues as before. Largest earthquakes since midnight had the magnitude of Mw3,3 and Mw3,0. A lot of smaller earthquake activity is currently happening and don&#8217;t always appears to be visible on the automatic map on Icelandic Met Office website. Over 200 earthquakes have taken place since midnight. Over 1200 earthquakes have taken place since 21st January 2020 when this started. Inflation remains the same and is now close to 50mm (GPS information can be viewed <a href=\"https:\/\/notendur.hi.is\/~hgeirs\/iceland_gps\/rnes\/rnes_100p.html\" rel=\"noopener noreferrer\" target=\"_blank\">here<\/a>). Rate of inflation seems to change slightly between days and I don&#8217;t know why that is happening. Most inflation seems to be happening close to the blue lagoon. Most of the earthquake activity is on a fault that is south-west to north-east direction and is south-east of highest point of the inflation. That makes a sense in terms of crust stress factors. What is missing is a earthquake swarm north of the main inflation area.<\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1645.png\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1645.png\" alt=\"\" width=\"540\" height=\"400\" class=\"aligncenter size-full wp-image-8259\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1645.png 540w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1645-300x222.png 300w\" sizes=\"auto, (max-width: 540px) 100vw, 540px\" \/><\/a><br \/>\nEarthquake activity in the Grindav\u00edk town area for the last 48 hours. <em>Copyright of this image belongs to Icelandic Met Office.<\/em><\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/Jar\u00f0skj\u00e1lftar-Grindav\u00edk-21.01.2020-til-02.02.2020.png\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/Jar\u00f0skj\u00e1lftar-Grindav\u00edk-21.01.2020-til-02.02.2020-1024x619.png\" alt=\"\" width=\"525\" height=\"317\" class=\"aligncenter size-large wp-image-8260\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/Jar\u00f0skj\u00e1lftar-Grindav\u00edk-21.01.2020-til-02.02.2020-1024x619.png 1024w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/Jar\u00f0skj\u00e1lftar-Grindav\u00edk-21.01.2020-til-02.02.2020-300x181.png 300w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/Jar\u00f0skj\u00e1lftar-Grindav\u00edk-21.01.2020-til-02.02.2020-768x464.png 768w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/Jar\u00f0skj\u00e1lftar-Grindav\u00edk-21.01.2020-til-02.02.2020.png 1119w\" sizes=\"auto, (max-width: 525px) 100vw, 525px\" \/><\/a><br \/>\nAll the earthquake activity in this area since 21st of January 2020 to 2nd February 2020. <em>Copyright of this image belongs to Icelandic Met Office.<\/em><\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/N\u00e1grenni-Grindav\u00edkur-sprungur-\u00e1-yfirbor\u00f0i-02.02.2020.jpg\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/N\u00e1grenni-Grindav\u00edkur-sprungur-\u00e1-yfirbor\u00f0i-02.02.2020-1024x616.jpg\" alt=\"\" width=\"525\" height=\"316\" class=\"aligncenter size-large wp-image-8261\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/N\u00e1grenni-Grindav\u00edkur-sprungur-\u00e1-yfirbor\u00f0i-02.02.2020-1024x616.jpg 1024w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/N\u00e1grenni-Grindav\u00edkur-sprungur-\u00e1-yfirbor\u00f0i-02.02.2020-300x180.jpg 300w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/N\u00e1grenni-Grindav\u00edkur-sprungur-\u00e1-yfirbor\u00f0i-02.02.2020-768x462.jpg 768w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/N\u00e1grenni-Grindav\u00edkur-sprungur-\u00e1-yfirbor\u00f0i-02.02.2020-1536x924.jpg 1536w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/N\u00e1grenni-Grindav\u00edkur-sprungur-\u00e1-yfirbor\u00f0i-02.02.2020.jpg 1570w\" sizes=\"auto, (max-width: 525px) 100vw, 525px\" \/><\/a><br \/>\nSurface image of the area that is now having earthquake swarms. <em>Copyright of this image belongs to Google. <\/em><\/p>\n<p><a href=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1550_trace.png\"><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1550_trace.png\" alt=\"\" width=\"540\" height=\"175\" class=\"aligncenter size-full wp-image-8262\" srcset=\"https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1550_trace.png 540w, https:\/\/icelandgeology.net\/wp-content\/uploads\/2020\/02\/200202_1550_trace-300x97.png 300w\" sizes=\"auto, (max-width: 540px) 100vw, 540px\" \/><\/a><br \/>\nThe earthquake activity in the last 48 hours. <em>Copyright of this image belongs to Icelandic Met Office.<\/em><\/p>\n<p>There are no signs of the magma that is now injecting it self into the crust at 3 to 6 km depth that has started to break up the surface. It is possible that pressure is not enough for that to happen just yet. What happens next is impossible to know for sure but earthquake activity is going to continue in this area until inflation stops or an eruption starts.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Donations Please remember to support my work with donations. I have removed all the advertisements because of increased tracking with those advertisements and almost no income from them. That means I am more dependant on donation to keep this website running. This is also important in times when there is a lot going on in &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/icelandgeology.net\/?p=8258\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Earthquake activity update for Grindav\u00edk town 2nd February 2020&#8221;<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[10,64,40,42,57,32,205],"tags":[],"class_list":["post-8258","post","type-post","status-publish","format-standard","hentry","category-earthquakes","category-magma","category-monitoring","category-reykjanes","category-swarm","category-volcano","category-thorbjorn"],"_links":{"self":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/8258","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=8258"}],"version-history":[{"count":1,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/8258\/revisions"}],"predecessor-version":[{"id":8263,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=\/wp\/v2\/posts\/8258\/revisions\/8263"}],"wp:attachment":[{"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=8258"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=8258"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/icelandgeology.net\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=8258"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}